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EV RESOURCES LTD — Capital/Financing Update 2023
Feb 26, 2023
64887_rns_2023-02-26_902843eb-f368-49d1-9b3b-3ec510572c65.pdf
Capital/Financing Update
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ASX ANNOUNCEMENT
27[th] February 2023
Tungsten Assays up to 15.9% W at the Christina Tungsten-Tin project
Highlights:
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A substantial mapping and sampling campaign at Christina has concluded with the balance 339 samples analysed.
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A 2,500m diamond drilling campaign has been planned to test down-dip extensions of mineralised quartz veins and interpreted structural trap sites.
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Assay results from sampling include Tungsten (W) values up to 15.9% and Tin (Sn) up to 1.41%. Best results include:
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Sample ZX23 7.60% W
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Sample ZX305 15.90% W
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oSample ZX424 3.49% WoSample ZX425 15.90% WoSample ZX426 3.65% WoSample ZX428 14.70% WoSample ZX/G13 4.59% W -
Mapping reveals a 1–3km wide, NW-SE trending zone of mineralised E-W striking quartz veins and micro vein swarms that extend for 8km from the northern boundary to the southern end of the concessions.
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Quartz vein density and assay results for W and Sn are highest in the central portion of the concessions and will be the target for most of the planned initial drilling.
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A Mining Licence has been issued over part of the 48km[2] project area, with final environmental permits imminent.
EV Resources Limited (“ EVR ”, or “ the Company ”) is pleased to report an update on the analytical results from a further 339 rock samples collected within the framework of a comprehensive sampling programme at the Christina Tin-Tungsten Project in Morocco, from locations on surface and underground.
A total of 439 samples have been collected from centimetre to metre-thick quartz veins, (some samples with visible wolframite and scheelite mineralisation), from millimetre to centimetrethick micro veins, and from the hosting two-mica granite in the immediate vicinity of the veins. Numerous veins from the most prospective segments of the concessions were mapped, surveyed and characterised.
Results from 100 of the 439 samples were reported on 17 November 2022 (refer ASX release “Further High Grade Results at the Christina Tin-Tungsten Project”) with the remaining 339 sample results reported in this announcement.
evresources.com.au
311-313 Hay St Subiaco, Western Australia 6008 +61 (0) 8 6489 0600 [email protected]
==> picture [480 x 314] intentionally omitted <==
Figure 1: Christina Project location, sample positions, tungsten assays, quartz veining
==> picture [455 x 298] intentionally omitted <==
Figure 2: Christina Project location, sample positions, tin assays, quartz veining
evresources.com.au
311-313 Hay St Subiaco, Western Australia 6008 +61 (0) 8 6489 0600 [email protected]
Geological Report
The Christina Tin (Sn) and Tungsten (W) grassroots exploration project is located approximately 120km east of Casablanca, Morocco. EVR has secured an option for a large area of 48 square kilometres under licence, a proportion of which has been converted to a Mining Licence.
The project area has seen sporadic mining during the 1930’s through to the early 1980’s, from a few nearly vertical shafts to 120m below surface and from at least three horizontal adits with lengths of up to 150m. Ore was hand-sorted and no plant was ever in operation. There has been no modern exploration undertaken within the concessions.
The deposit is located in the southern part of the Hercynian granitic Zaer intrusive complex. Mineralisation is associated with a coarse-grained two-mica granite, frequently greisenised and showing potassic alteration, and hosting a locally high density of quartzose micro veins.
Mapping of structure and geology initially focused on the better-known central areas of the concessions (see Figure 1), where most of the historical mining and extraction had occurred. Mapping and sampling activities were subsequently extended to the north and south, and in the process outlining multiple mineralised veins that apparently had previously never been explored or mined.
Mapping has demonstrated a NW-SE trending, 1 to 3 kilometre wide corridor of approximately E-W striking quartz veins and micro veins that are frequently mineralised. There are very few veins striking in directions other than E-W. The SW part of the concessions is underlain by biotite granite that appears to have less prospectivity for mineralisation. The north-eastern and eastern parts of the concessions, although underlain by the highly prospective two-mica granite, were not investigated at this stage due to agricultural cover.
Analytical Results
Table 1 shows a compilation of assays of Tungsten and Tin elements in all 439 samples collected during the entire mapping and sampling programme. Sample numbers, descriptions and coordinates for the latest batch of 339 samples are highlighted in light blue.
Tungsten (W) :
Of the 339 samples collected from quartz veins at the Christina Project, 22 recorded values in
For the 439 samples collected in total during the programme, 36 samples recorded values >1% W (including four samples exceeding the upper XRF detection limit of 15.9% W), plus another 51 samples with values ranging between 0.1 to 1% W. The average value for all 439 samples calculates at 0.45% W, including barren granite samples.
Tin (Sn) :
Of the 339 new samples, 6 recorded values >0.5% Sn, with a maximum of 1.4% Sn, while another 23 samples recorded values in a range of 0.1 to 0.5% Sn.
For the 439 samples collected in total, six samples recorded >0.5% Sn, and 37 values >0.1 to 0.5% Sn. The averaged value for all 439 samples calculates at 0.04% Sn, including barren granite samples.
evresources.com.au
311-313 Hay St Subiaco, Western Australia 6008 +61 (0) 8 6489 0600 [email protected]
Next Steps
A reconnaissance-style diamond exploration programme of approximately 2,500 metres has been designed to test down-dip extensions of mineralised quartz veins, and to drill into interpreted structural traps potentially hosting mineralisation.
Under EVR’s agreement to acquire the Christine Project, EVR holds the right to exercise its option to acquire 60% of Skiait Mining, the 100% owner of Sokhret Allal Tin-Tungsten ‘Christina’ Project. (See ASX Announcement dated 26[th] May 2022 “ EVR to Acquire Christina Tin - Tungsten Project in Morocco ”).
The Company has been advised that the final environmental permit for the Mining Licence is imminent. Drilling will commence as soon as possible after that permit is received.
Upcoming News
It is anticipated that the following activities will take place on the Christina Project over the next few months, subject to changes or delays which may be out of the Company’s control.
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March 2023 – Grant of environmental permit
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April 2023 – Commencement of drilling
ENDS
For further information, please contact:
Luke Martino Adrian Paul Non-Executive Chairman Executive Director Tel: +61 8 6489 0600 Tel: +61 8 6489 0600 E: [email protected] E: [email protected]
This ASX announcement was authorised for release by the Board of EV Resources Limited.
Forward Looking Statement
Forward Looking Statements regarding EVR´s plans with respect to its mineral properties and programmes are forward-looking statements. There can be no assurance that EVR’s plans for development of its mineral properties will proceed as currently expected. There can also be no assurance that EVR will be able to confirm the presence of additional mineral resources, that any mineralisation will prove to be economic or that a mine will successfully be developed on any of EVR’s mineral properties. The performance of EVR may be influenced by a number of factors which are outside the control of the Company and its Directors, staff, and contractors. These statements include, but are not limited to statements regarding future production, resources or reserves and exploration results. All of such statements are subject to certain risks and uncertainties, many of which are difficult to predict and generally beyond the control of the company, that could cause actual results to differ materially from those expressed in, or implied or projected by, the forward-looking information and statements. These risks and uncertainties include, but are not limited to: (i) those relating to the interpretation of drill results, the geology, grade and continuity of mineral deposits and conclusions of economic evaluations, (ii) risks relating to possible variations in reserves, grade, planned mining dilution and ore loss, or recovery rates and changes in project parameters as plans continue to be refined, (iii) the potential for delays in exploration or development activities or the completion of feasibility studies, (iv) risks related to commodity price and foreign exchange rate fluctuations, (v) risks related to failure to obtain adequate financing on a timely basis and on acceptable terms or delays in obtaining governmental approvals or in the completion of development or construction activities, and (vi) other risks and uncertainties related to the company’s prospects, properties and business strategy. Our audience is cautioned not to place undue reliance on these forward-looking statements that speak only as of the date hereof, and we do not undertake any obligation to revise and disseminate forward-looking statements to reflect events or circumstances after the date hereof, or to reflect the occurrence of or non-occurrence of any events.
evresources.com.au
311-313 Hay St Subiaco, Western Australia 6008 +61 (0) 8 6489 0600 [email protected]
Competent Person’s Statement
The information in this release that relates to Exploration Results is based on information compiled by Mr Baker Khudeira who is a Member of the Australian Institute of Mining and Metallurgy (MAusIMM Number 230652). Mr Khudeira is a consultant to EVR. Mr Khudeira has sufficient experience which is relevant to the style of mineralisation and type of deposit under consideration and to the activity which he is undertaking to qualify as a Competent Person as defined in the 2012 Edition of the “Australasian Code for Reporting of Exploration Results, Mineral Resources and Ore Reserves”. Mr Khudeira consents to the inclusion in this announcement of the matters based on information in the form and context in which it appears
Compliance Statement
This announcement contains information on the Christina Tungsten-Tin Project extracted from an ASX market announcements dated 21 September 2022 and 17 November 2022 and reported in accordance with the 2012 edition of the “Australasian Code for Reporting of Exploration Results, Mineral Resources and Ore Reserves” ("2012 JORC Code"). EVR confirms that it is not aware of any new information or data that materially affects the information included in the original ASX market announcement.
Table 1. Assay Results for 439 Samples from the Christina Project
| Sample No. |
Description | Easting | Northing | Sn | W |
|---|---|---|---|---|---|
| w= wolframite; sch= scheelite; fsp= feldspar | X | Y | ppm | ppm | |
| ZX 001 | major vein from trench, with w | -6.742668 | 33.194482 | 2500 | 19850 |
| ZX 002 | major vein from trench level, greyish quartz with w | -6.742917 | 33.194553 | 490 | 23900 |
| ZX 003 | massive quartz vein, 130cm, traces of w | -6.743308 | 33.194587 | 130 | 32 |
| ZX 004 | quartz vein, 40cm, finely disseminated w? | -6.741815 | 33.194565 | 17 | 12 |
| ZX 005 | 40cm wide corridor of quartz, granite, traces of w (2,5m distance from ZX004) |
-6.741811 | 33.194534 | 29 | 34 |
| ZX 006 | anastomosing quartz veins, 4-48cm, minor w | -6.743372 | 33.194604 | 918 | 4730 |
| ZX 007 | quartz vein, traces of w | -6.743678 | 33.194711 | 4150 | 593 |
| ZX 008 | quartz vein, 1cm | -6.744520 | 33.194600 | 25 | 7 |
| ZX 009 | quartz vein, w | -6.744955 | 33.195192 | 2950 | 21900 |
| ZX 010 | quartz vein, 1,5cm | -6.745090 | 33.194380 | 25 | 21 |
| ZX 011 | quartz vein, traces of w | -6.745950 | 33.195378 | 759 | 976 |
| ZX 012 | quartz, mica and fsp vein structure, not mineralised; crosscuted by fracture (N40E) |
-6.745278 | 33.194086 | 19 | 20 |
| ZX 013 | quartz vein, with w | -6.746088 | 33.195635 | 153 | 14 |
| ZX 014 | grey quartz lens, up to 15cm, millimetric w | -6.745227 | 33.194290 | 160 | 21100 |
| ZX 015 | quartz vein, traces of w | -6.746634 | 33.195688 | 43 | 13 |
| ZX 016 | quartz vein, traces of w, corresponds to a system of veins of 1-10cm | -6.745534 | 33.194494 | 3860 | 241 |
| ZX 017 | quartz vein, with w | -6.746836 | 33.195416 | 2010 | 29900 |
| ZX 018 | quartz, muscovite and fsp vein, 5cm | -6.745937 | 33.194595 | 31 | 19 |
| ZX 019 | quartz vein in granite | -6.745178 | 33.194162 | 31 | 18 |
| ZX 020 | quartz vein in granite | -6.745658 | 33.193993 | 41 | 29 |
| ZX 021 | quartz vein, with w | -6.747281 | 33.195423 | 240 | 12250 |
| ZX 022 | brecciated grey quartz vein, up to 40cm, traces of millimetric w and sch |
-6.746979 | 33.195670 | 17 | 18 |
| ZX 023 | quartz vein, with w | -6.747857 | 33.195453 | 7250 | 76000 |
| ZX 024 | grey-white quartz vein structure, 3-11cm, with geodes | -6.747711 | 33.195760 | 38 | 27 |
| ZX 025 | quartz vein, traces of w | -6.748469 | 33.195514 | 17 | 17 |
| ZX 026 | lenticular structure with quartz, mica and fsp, 2-3cm | -6.748800 | 33.195694 | 28 | 16 |
| ZX 027 | quartz vein, traces of w | -6.748330 | 33.195347 | 72 | 29 |
| ZX 028 | quartz vein, with granite breccia, 56cm | -6.747723 | 33.195158 | 92 | 29 |
| ZX 029 | mineralised veins with quartz, oxidised | -6.748750 | 33.195312 | 544 | 564 |
| ZX 030 | grey quartz vein, brecciated, with w and malachite, 34cm | -6.747525 | 33.194942 | 571 | 708 |
| ZX 031 | faintly mineralised veins with quartz, oxidised | -6.749125 | 33.195390 | 12 | 17 |
| ZX 032 | granitic host rock | -6.747756 | 33.195227 | 17 | 6 |
| ZX 033 | granitic host rock | -6.749117 | 33.195223 | 23 | 24 |
| ZX 034 | grey quartz vein, brecciated, with w and malachite, 34cm | -6.747952 | 33.194966 | 2110 | 16850 |
evresources.com.au
311-313 Hay St Subiaco, Western Australia 6008 +61 (0) 8 6489 0600 [email protected]
| Sample No. |
Description | Easting | Northing | Sn | W | |
| w= wolframite; sch= scheelite; fsp= feldspar | X | Y | ppm | ppm | ||
| ZX 035 | faintly mineralised veins with quartz, oxidised | -6.749536 | 33.195600 | 44 | 82 | |
| ZX 036 | massive quartz vein, up to 10cm | -6.748463 | 33.195006 | 32 | 11 | |
| ZX 037 | mineralised veins with quartz, oxidised | -6.750170 | 33.195862 | 240 | 2550 | |
| ZX 038 | grey quartz vein, lenticular, 3-20cm | -6.748609 | 33.194937 | 105 | 2620 | |
| ZX 039 | quartz vein, 3-15cm, vein walls are are greisenised | -6.749269 | 33.195009 | 445 | 42 | |
| ZX 040 | quartz veins, traces of w, oxidised | -6.749698 | 33.195130 | 20 | 30 | |
| ZX 041 | 2 quartz veins, traces of w, oxidised | -6.749985 | 33.194893 | 23 | 4 | |
| ZX 042 | grey quartz, oxidation | -6.750442 | 33.195102 | 25 | 92 | |
| ZX 043 | quartz veins, traces of w, oxidised | -6.750036 | 33.195050 | 12 | 5 | |
| ZX 044 | grey quartz, 5cm, croscuted by fault N170 | -6.746815 | 33.194636 | 180 | 929 | |
| ZX 045 | quartz vein, w | -6.747567 | 33.194582 | 180 | 21200 | |
| ZX 046 | grey quartz, 5cm | -6.747145 | 33.194712 | 84 | 8 | |
| ZX 047 | quartz veins, oxidation | -6.748344 | 33.194492 | 3450 | 1855 | |
| ZX 048 | quartz vein, 3cm | -6.747662 | 33.194752 | 20 | 19 | |
| ZX 049 | quartz veins, traces of oxidation | -6.749888 | 33.194600 | 17 | 16 | |
| ZX 050 | pegmatite with quartz, feldspar and micas, 4cm | -6.745774 | 33.193527 | 15 | 3 | |
| ZX 051 | quartz vein with traces of iron oxides | -6.750133 | 33.194721 | 203 | 9 | |
| ZX 052 | quartz, some w | -6.746342 | 33.193578 | 104 | 249 | |
| ZX 053 | quartz vein, traces of iron oxides | -6.744718 | 33.193566 | 394 | 49 | |
| ZX 054 | quartz vein, traces of cassiterite | -6.746115 | 33.193548 | 7010 | 25 | |
| ZX 055 | quartz vein with iron oxides | -6.744905 | 33.193926 | 18 | 5 | |
| ZX 056 | granitic host rock | -6.746284 | 33.193621 | 15 | 2 | |
| ZX 057 | quartz vein with iron oxides | -6.745164 | 33.193467 | 282 | 8230 | |
| ZX 058 | granitic host rock | -6.746380 | 33.193511 | 16 | 9 | |
| ZX 059 | quartz vein with iron oxides | -6.747060 | 33.195480 | 25 | 17 | |
| ZX 060 | quartz vein with iron oxides | -6.744351 | 33.193109 | 57 | 17 | |
| ZX 061 | quartz-iron oxides, tension gashes | -6.745874 | 33.193624 | 505 | 938 | |
| ZX 062 | quartz vein with iron oxides | -6.743709 | 33.193288 | 15 | 4 | |
| ZX 063 | granitic host rock | -6.745874 | 33.193735 | 14 | 19 | |
| ZX 064 | quartz, slight oxidation | -6.745302 | 33.192648 | 724 | 188 | |
| ZX 065 | granitic host rock | -6.746115 | 33.193653 | 16 | 5 | |
| ZX 066 | quartz vein with iron oxides | -6.743156 | 33.192888 | 25 | 34 | |
| ZX 067 | quartz vein with iron oxides | -6.746426 | 33.193746 | 288 | 4 | |
| ZX 068 | quartz vein with iron oxides | -6.744647 | 33.192641 | 2930 | 1400 | |
| ZX 069 | quartz vein with iron oxides | -6.746094 | 33.193879 | 34 | 24 | |
| ZX 070 | quartz vein with iron oxides | -6.743780 | 33.192913 | 30 | 8 | |
| ZX 071 | mineralized veins with quartz and oxidation | -6.747180 | 33.194201 | 330 | 9190 | |
| ZX 072 | granitic host rock | -6.744149 | 33.193083 | 18 | 1 | |
| ZX 073 | quartz vein with iron oxides | -6.746743 | 33.193701 | 2380 | 1035 | |
| ZX 074 | pegmatite with quartz, fsp and micas, 3cm | -6.744025 | 33.192211 | 19 | 9 | |
| ZX 075 | mineralized veins with quartz and oxidation | -6.744046 | 33.192527 | 279 | 2580 | |
| ZX 076 | quartz vein, 10cm, 4 m in length | -6.743487 | 33.192048 | 3770 | 214 | |
| ZX 077 | quartz vein with iron oxides | -6.743518 | 33.192629 | 25 | 9 | |
| ZX 078 | granitic host rock, cut by fractures (F1 : N70E; F2 : N30E) | -6.743448 | 33.192469 | 23 | 8 | |
| ZX 079 | quartz vein with iron oxides | -6.742840 | 33.192538 | 27 | 45 | |
| ZX 080 | grey quartz, w (5mm aggregate), 10cm | -6.743381 | 33.192194 | 598 | 902 | |
| ZX 081 | pegmatite with quartz, 10cm | -6.743281 | 33.192780 | 43 | 5 | |
| ZX 082 | quartz vein with iron oxides | -6.746421 | 33.193273 | 17 | 8 | |
| ZX 083 | granitic host rock | -6.742805 | 33.192846 | 17 | 6 |
evresources.com.au
311-313 Hay St Subiaco, Western Australia 6008 +61 (0) 8 6489 0600 [email protected]
| Sample No. |
Description | Easting | Northing | Sn | W | |
| w= wolframite; sch= scheelite; fsp= feldspar | X | Y | ppm | ppm | ||
| ZX 084 | quartz vein with iron oxides | -6.746920 | 33.193273 | 12 | 5 | |
| ZX 085 | quartz, with iron oxidation, 20cm | -6.747246 | 33.193245 | 59 | 32 | |
| ZX 086 | grey quartz, traces of w, 2cm | -6.747643 | 33.193149 | 21 | 30 | |
| ZX 087 | quartz vein with iron oxides | -6.747254 | 33.193597 | 342 | 34 | |
| ZX 088 | grey quartz vein, 2cm, intersected by N-S fracture | -6.748103 | 33.193192 | 17 | 16 | |
| ZX 089 | mineralized veins with quartz and oxidation | -6.747176 | 33.193539 | 19 | 187 | |
| ZX 090 | granitic host rock | -6.747783 | 33.193400 | 14 | 3 | |
| ZX 091 | mineralized veins with quartz and oxidation | -6.744030 | 33.196270 | 850 | 14 | |
| ZX 092 | granitic host rock | -6.748660 | 33.196070 | 16 | 6 | |
| ZX 093 | quartz vein with iron oxides, 50cm | -6.746064 | 33.197905 | 4 | 19 | |
| ZX 094 | veins with iron oxides and indicatopn of w, 5cm | -6.753334 | 33.200139 | 32 | 9 | |
| ZX 095 | parallel veins of quartz, 3cm | -6.754156 | 33.199262 | 41 | 52 | |
| ZX 096 | parallel veins of quartz within brecciated granite of 5-10 cm | -6.752330 | 33.200488 | 45 | 5 | |
| ZX 097 | quartz vein, 6cm | -6.752015 | 33.201159 | 3240 | 9010 | |
| ZX 098 | major vein in trench, greyish quartz, traces of w | -6.759325 | 33.198487 | 283 | 279 | |
| ZX 099 | major quartz vein with iron oxidation | -6.748748 | 33.200566 | 412 | 44 | |
| ZX 100 | major quartz vein with iron oxidation, > 30cm | -6.752078 | 33.197410 | 4 | 42 | |
| ZX 101 | two quartz veins with iron oxidation, < 2cm | -6.751006 | 33.197933 | 6 | 5 | |
| ZX 102 | grey granite with muscovite and biotite | -6.751490 | 33.197774 | 11 | 15 | |
| ZX 103 | massive granite, two micas | -6.749149 | 33.198691 | 20 | 10 | |
| ZX 104 | quartz veins, 3-5cm, w | -6.746496 | 33.200228 | 46 | 5030 | |
| ZX 105 | quartz vein, w, granite | -6.745233 | 33.200936 | 4030 | 74300 | |
| ZX 106 | quartz vein, with malachite and iron oxides | -6.745207 | 33.200921 | 1370 | 985 | |
| ZX 107 | quartz micro vein | -6.744199 | 33.200826 | 31 | 22 | |
| ZX 108 | quartz vein with iron oxides, two-mica granite, indication of malachite | -6.747685 | 33.198111 | 133 | 67 | |
| ZX 109 | three grey quartz veins @ 2cm | -6.750147 | 33.202116 | 20 | 19 | |
| ZX 110 | quartz vein, 2-3cm, within granitic host rock | -6.747965 | 33.201022 | 19 | 20 | |
| ZX 111 | quartz vein, > 20cm | -6.747586 | 33.200788 | 2 | 264 | |
| ZX 112 | quartz vein, 1-3cm | -6.747272 | 33.200796 | 84 | 39 | |
| ZX 113 | quartz vein, 3-5cm, oxidised | -6.748029 | 33.200900 | 45 | 37 | |
| ZX 114 | two quartz veins, traces of w, in granite | -6.748860 | 33.199054 | 11 | 187 | |
| ZX 115 | major vein with grey quartz and w, 80cm | -6.752778 | 33.198887 | 270 | 601 | |
| ZX 116 | major quartz vein, w, 70 cm | -6.753349 | 33.198946 | 2110 | 28400 | |
| ZX 117 | quartz vein, 15cm | -6.753854 | 33.198448 | 20 | 9 | |
| ZX 118 | quartz vein, 4cm | -6.754291 | 33.197460 | 168 | 20 | |
| ZX 119 | quartz vein, 12cm | -6.752872 | 33.197883 | 16 | 6 | |
| ZX 120 | major vein with grey quartz and oxides, pyrite, 70cm | -6.754448 | 33.201714 | 50 | 12750 | |
| ZX 121 | quartz vein, 27cm | -6.756435 | 33.200314 | 34 | 51 | |
| ZX 122 | quartz vein, traces of w, 4-8cm | -6.757215 | 33.199443 | 176 | 268 | |
| ZX 123 | major vein, 60cm | -6.756860 | 33.197746 | 4 | 2 | |
| ZX 124 | massive quartz vein, 5cm | -6.755570 | 33.197281 | 522 | 24 | |
| ZX 125 | quartz vein, 7cm | -6.756152 | 33.197230 | 32 | 86 | |
| ZX 126 | massive quartz vein, w, 20cm | -6.755256 | 33.199134 | 1170 | 11800 0 |
|
| ZX 127 | major vein in trench, w, 80cm | -6.758174 | 33.197047 | 2390 | 13200 | |
| ZX 128 | lens structure with grey quartz, up to 20cm | -6.759620 | 33.197565 | 26 | 18 | |
| ZX 129 | major vein, 100cm | -6.760299 | 33.197761 | 31 | 17 | |
| ZX 130 | quartz vein, oxidised, 12cm | -6.756644 | 33.196435 | 48 | 14 | |
| ZX 131 | quartz vein, 10cm, w, iron oxide | -6.757104 | 33.195930 | 1845 | 7610 | |
| ZX 132 | quartz vein, 12cm, iron oxide | -6.757058 | 33.196175 | 411 | 458 |
evresources.com.au
311-313 Hay St Subiaco, Western Australia 6008 +61 (0) 8 6489 0600 [email protected]
| Sample No. |
Description | Easting | Northing | Sn | W | |
| w= wolframite; sch= scheelite; fsp= feldspar | X | Y | ppm | ppm | ||
| ZX 133 | micro-vein, 2cm, w, iron oxide | -6.757510 | 33.196199 | 1455 | 9560 | |
| ZX 134 | quartz vein, 10cm, iron oxide | -6.757629 | 33.195971 | 40 | 36 | |
| ZX 135 | quartz vein, 12cm, iron oxide | -6.759213 | 33.195563 | 4 | 33 | |
| ZX 136 | quartz vein, 7cm, iron oxide | -6.759310 | 33.195675 | 10 | 11 | |
| ZX 137 | micro-vein, 7cm, grey quartz, iron oxide | -6.759474 | 33.196061 | 8 | 5 | |
| ZX 138 | micro-vein, 7cm, grey quartz, iron oxide | -6.757904 | 33.196403 | 305 | 560 | |
| ZX 139 | Vein of 20 cm gray quartz and iron oxide | -6.761137 | 33.192787 | 31 | 6 | |
| ZX 140 | quartz vein, 30cm, w, iron oxide | -6.754432 | 33.193068 | 3760 | 7160 | |
| ZX 141 | granite | -6.755741 | 33.193386 | 15 | 3 | |
| ZX 142 | granite | -6.755752 | 33.193413 | 15 | 5 | |
| ZX 143 | micro-vein, 3cm, grey quartz, iron oxide | -6.755769 | 33.193322 | 42 | 815 | |
| ZX 144 | major vein with grey quartz, w and malachite, 50cm | -6.758010 | 33.193232 | 91 | 5610 | |
| ZX 145 | micro-vein with quartz and iron oxidation | -6.752628 | 33.191348 | 4 | 11 | |
| ZX 146 | micro-vein with quartz and iron oxidation | -6.753256 | 33.191018 | 4 | 4 | |
| ZX 147 | micro-vein with quartz and iron oxidation | -6.754913 | 33.190037 | 6 | 12 | |
| ZX 148 | corridor of micro veins, with quartz and iron oxidation | -6.755087 | 33.190103 | 3 | 3 | |
| ZX 149 | micro-vein with quartz and iron oxidation | -6.754971 | 33.189951 | 52 | 5 | |
| ZX 150 | micro-vein with quartz and iron oxidation | -6.755324 | 33.189938 | 7 | 3 | |
| ZX 151 | micro-vein with quartz and iron oxidation | -6.756089 | 33.190071 | 16 | 6 | |
| ZX 152 | major vein with grey quartz, w, 65cm | -6.749541 | 33.193528 | 1440 | 15900 0 |
|
| ZX 153 | major vein with grey quartz, w, 50cm | -6.752055 | 33.192106 | 597 | 5860 | |
| ZX 154 | micro-vein with quartz and iron oxidation | -6.753986 | 33.190669 | 2 | 6 | |
| ZX 155 | micro-vein with quartz and iron oxidation | -6.755697 | 33.189840 | 21 | 27 | |
| ZX 156 | micro-vein with quartz and iron oxidation | -6.756094 | 33.189297 | 28 | 84 | |
| ZX 157 | major vein with grey quartz, w, 50cm | -6.757621 | 33.186114 | 3410 | 15900 0 |
|
| ZX 158 | quartz veins, oxidised | -6.758024 | 33.186938 | 80 | 56700 | |
| ZX 159 | major vein with grey quartz, some w, 50cm | -6.758935 | 33.187875 | 283 | 1920 | |
| ZX 160 | major vein with grey quartz, traces of w, iron oxides, 60cm | -6.745006 | 33.191595 | 23 | 62 | |
| ZX 161 | micro-vein with quartz, w, 5cm, heavily veined within 3-5m | -6.745907 | 33.191378 | 26 | 8700 | |
| ZX 162 | major vein, network of micro-veins in granite, traces of w, iron oxides, 60cm |
-6.742508 | 33.190990 | 91 | 22 | |
| ZX 163 | micro-vein in coarse pink granite, 3cm | -6.741961 | 33.191326 | 17 | 10 | |
| ZX 164 | micro-vein, indication of w, 5-10cm, in tension gash | -6.739445 | 33.193556 | 24 | 10 | |
| ZX 165 | major vein, network of micro-veins in granite, iron oxides, corridor width of 4m |
-6.736465 | 33.193155 | 7 | 30 | |
| ZX 166 | major vein, traces of w, iron oxides, 40cm | -6.734147 | 33.193008 | 498 | 24 | |
| ZX 167 | micro-vein filling, 3-5cm | -6.731586 | 33.193644 | 8 | 20 | |
| ZX 168 | major vein, 50cm | -6.759567 | 33.188928 | 16 | 10 | |
| ZX 169 | major vein, 50cm | -6.762200 | 33.192730 | 222 | 15 | |
| ZX 170 | quartz vein, with iron oxides | -6.758986 | 33.190352 | 49 | 10 | |
| ZX 171 | tension gash, with quartz, iron oxidation, w | -6.758054 | 33.190379 | 12 | 1905 | |
| ZX 172 | quartz vein, oxidised | -6.756862 | 33.190465 | 14 | 6 | |
| ZX 173 | quartz vein, oxidised | -6.754294 | 33.189149 | 11 | 50 | |
| ZX 174 | major vein, grey quartz, iron oxides, 10cm | -6.751223 | 33.201097 | 75 | 10 | |
| ZX 175 | micro quartz vein, with oxidation, 1,5cm | -6.751362 | 33.201179 | 21 | 4 | |
| ZX 176 | micro vein, with quartz and iron oxidation, 1cm | -6.749850 | 33.200437 | 364 | 96 | |
| ZX 177 | quartz vein, w, oxidised, malachite coating, 7cm | -6.749490 | 33.200030 | 5220 | 12200 | |
| ZX 178 | quartz vein, iron oxidation, 6cm | -6.750200 | 33.201200 | 59 | 26 | |
| ZX 179 | quartz vein, oxidised | -6.750820 | 33.202430 | 26 | 8 | |
| ZX 180 | major vein (#1), frequent traces of w, 65cm | -6.737788 | 33.197780 | 1 | 2 |
evresources.com.au
311-313 Hay St Subiaco, Western Australia 6008 +61 (0) 8 6489 0600 [email protected]
| Sample No. |
Description | Easting | Northing | Sn | W | |
| w= wolframite; sch= scheelite; fsp= feldspar | X | Y | ppm | ppm | ||
| ZX 181 | major vein (#1), frequent traces of w, 50cm | -6.736567 | 33.197054 | 1 | 4 | |
| ZX 182 | major vein (#2), with brecciated quartz and pyrite and iron oxides, 70cm |
-6.738037 | 33.196651 | 21 | 4 | |
| ZX 183 | major vein (#2), with brecciated quartz and pyrite and iron oxides, 100cm |
-6.735219 | 33.196022 | 9 | 5 | |
| ZX 184 | major vein (#1), 50cm | -6.735211 | 33.196379 | 2 | 15 | |
| ZX 185 | granite between major veins #1 and #2 | -6.735664 | 33.196675 | 15 | 3 | |
| ZX 186 | granite between major veins #1 and #2 | -6.734635 | 33.195787 | 14 | 2 | |
| ZX 187 | major vein (#2) occurring as corridor of veins with quartz, pyrite and iron oxides, 100cm |
-6.733652 | 33.195823 | 19 | 4 | |
| ZX 188 | micro-veins with pyrite and iron oxides, 15cm | -6.753796 | 33.188564 | 9 | 12 | |
| ZX 189 | quartz vein, 20cm | -6.754468 | 33.188024 | 30 | 6 | |
| ZX 190 | micro-veins, 3-10cm | -6.754259 | 33.187532 | 25 | 8 | |
| ZX 191 | major vein, iron oxides, 100cm | -6.758917 | 33.194163 | 1 | 18 | |
| ZX 192 | major vein, iron oxides, 40cm | -6.761055 | 33.194265 | 73 | 35 | |
| ZX 193 | quartz vein, iron oxides, 20cm | -6.760363 | 33.195102 | 11 | 15 | |
| ZX 194 | quartz vein, iron oxides, muscovite, 30cm | -6.761237 | 33.196450 | 6 | 7 | |
| ZX 195 | major vein, iron oxides, 100cm | -6.760960 | 33.195556 | 1 | 7 | |
| ZX 196 | corridor of veins, iron oxides, w and probably sch, 10cm | -6.762471 | 33.195505 | 300 | 37200 | |
| ZX 197 | corridor of veins, iron oxides, w, traces of malachite, 200cm | -6.764518 | 33.195538 | 300 | 16100 | |
| ZX 198 | major vein, iron oxides,w, 60cm | -6.763344 | 33.194354 | 430 | 15100 | |
| ZX 199 | quartz veins, iron oxides, 25cm | -6.765200 | 33.193953 | 4 | 3 | |
| ZX 200 | major vein, iron oxides, 80cm | -6.763952 | 33.196438 | 63 | 4 | |
| ZX 201 | major vein, iron oxides, 100cm | -6.765960 | 33.196761 | 7 | 45 | |
| ZX 202 | quartz vein, 3cm | -6.754389 | 33.197252 | 89 | 112 | |
| ZX 203 | quartz vein, 15cm | -6.754666 | 33.197451 | 3 | 4 | |
| ZX 204 | quartz vein, traces of iron oxide, w, 5cm | -6.755696 | 33.199188 | 1360 | 24500 | |
| ZX 205 | major vein, some w, 100cm | -6.757181 | 33.196647 | 287 | 3660 | |
| ZX 206 | quartz vein, 1-12cm | -6.756872 | 33.197189 | 3 | 9 | |
| ZX 207 | major vein, w, 60cm | -6.756146 | 33.196941 | 1205 | 3880 | |
| ZX 208 | quartz vein, w, 7-20cm | -6.757816 | 33.195762 | 14050 | 6450 | |
| ZX 209 | granitic host, 3m N of ZX208 | -6.757813 | 33.195744 | 18 | 5 | |
| ZX 210 | granitic host, 3m S of ZX208 | -6.757820 | 33.195835 | 16 | 4 | |
| ZX 211 | quartz vein, 5-10cm | -6.758460 | 33.195603 | 3 | 26 | |
| ZX 212 | quartz vein, traces of iron oxide, 15cm | -6.752884 | 33.199137 | 23 | 4 | |
| ZX 213 | major vein, 80cm, some sulphides | -6.759622 | 33.193120 | 26 | 9 | |
| ZX 214 | major vein, 70cm | -6.760388 | 33.193299 | 135 | 60 | |
| ZX 215 | major vein, 60cm, iron oxides | -6.760983 | 33.193263 | 364 | 14 | |
| ZX 216 | major vein, 50cm | -6.761778 | 33.193078 | 3 | 44 | |
| ZX 217 | major vein, white quartz, iron oxides | -6.736441 | 33.190227 | 12 | 59 | |
| ZX 218 | major vein, white quartz, iron oxides | -6.735684 | 33.189536 | 7 | 4 | |
| ZX 219 | major vein, white quartz, iron oxides | -6.736028 | 33.188706 | 1055 | 55 | |
| ZX 220 | major vein, white quartz, iron oxides | -6.737319 | 33.188331 | 17 | 6 | |
| ZX 221 | major vein, white quartz, iron oxides, dextral movement | -6.737707 | 33.187734 | 28 | 5 | |
| ZX 222 | major vein, white quartz, iron oxides | -6.734337 | 33.188769 | 2 | 2 | |
| ZX 223 | major vein, white quartz, iron oxides | -6.733298 | 33.189693 | 10 | 14 | |
| ZX 224 | major vein, white quartz, iron oxides | -6.737502 | 33.189481 | 3200 | 16 | |
| ZX 225 | micro-vein, 3cm, iron oxides | -6.751133 | 33.186227 | 22 | 17 | |
| ZX 226 | micro-vein, 3cm, rare w, iron oxides | -6.750430 | 33.185769 | 25 | 342 | |
| ZX 227 | quartz vein, 8-10cm, masive w, sulphides and iron oxides | -6.751138 | 33.186015 | 290 | 21700 | |
| ZX 228 | quartz vein, 10cm | -6.752355 | 33.185221 | 63 | 21 |
evresources.com.au
311-313 Hay St Subiaco, Western Australia 6008 +61 (0) 8 6489 0600 [email protected]
| Sample No. |
Description | Easting | Northing | Sn | W | |
| w= wolframite; sch= scheelite; fsp= feldspar | X | Y | ppm | ppm | ||
| ZX 229 | major vein, brecciated quartz and iron oxides | -6.754745 | 33.182675 | 12 | 9 | |
| ZX 230 | quartz vein, large muscovite flakes and orthoclase clasts, 1m corridor with multiple veins |
-6.756245 | 33.182204 | 13 | 7 | |
| ZX 231 | micro-vein, iron oxides | -6.754993 | 33.181708 | 2 | 3 | |
| ZX 232 | micro-vein, iron oxides | -6.751875 | 33.181886 | 7 | 63 | |
| ZX 235 | major vein, iron oxides, 60cm | -6.767420 | 33.196886 | 2 | 16 | |
| ZX 236 | cm-thick vein, 2-3cm | -6.765473 | 33.198522 | 8 | 9 | |
| ZX 237 | tension gash with quartz and traces of iron oxides, 15cm | -6.765198 | 33.200413 | 1270 | 2130 | |
| ZX 238 | quartz vein array, iron oxides, average 10cm | -6.765058 | 33.200832 | 8 | 548 | |
| ZX 239 | quartz vein, iron oxides, pyrite stains, w, 15cm | -6.765223 | 33.201239 | 30 | 4560 | |
| ZX 240 | quartz vein, iron oxides, w, intense hydrothermal alteration, 10cm | -6.762991 | 33.200836 | 320 | 4470 | |
| ZX 241 | quartz vein, iron oxides, w, intense hydrothermal alteration, 5cm | -6.763570 | 33.200453 | 1790 | 332 | |
| ZX 242 | network of quartz veins, iron oxides, 5cm average | -6.764266 | 33.200971 | 3 | 3 | |
| ZX 243 | quartz vein, traces of iron oxide, 10-20cm | -6.753268 | 33.199336 | 138 | 26 | |
| ZX 244 | anastomosing quartz veins, traces of w, 2-10cm | -6.754052 | 33.199921 | 471 | 1055 | |
| ZX 245 | quartz vein, 3-7cm | -6.755148 | 33.199812 | 12 | 5 | |
| ZX 246 | quartz vein, rare w, 10-15cm | -6.755249 | 33.200975 | 30 | 1025 | |
| ZX 247 | major vein, 35cm | -6.755935 | 33.200509 | 17 | 22 | |
| ZX 248 | major vein, 30cm | -6.759986 | 33.199566 | 2 | 3 | |
| ZX 249 | quartz vein, w, 4cm | -6.760032 | 33.199784 | 616 | 5140 | |
| ZX 250 | quartz vein, iron oxides, rare w, 10cm | -6.760090 | 33.200812 | 135 | 102 | |
| ZX 251 | quartz vein, feldspar clasts, w, 10cm | -6.761138 | 33.201113 | 1330 | 21500 | |
| ZX 252 | quartz vein, traces of iron oxides, some w, 1-8cm | -6.761084 | 33.201504 | 82 | 764 | |
| ZX 253 | major vein, 80cm, iron oxides | -6.917475 | 32.899586 | 4 | 3 | |
| ZX 254 | micro-vein, 6cm | -6.740154 | 33.203102 | 8 | 7 | |
| ZX 255 | micro-vein, 4cm, iron oxides | -6.740735 | 33.204094 | 48 | 16 | |
| ZX 256 | major vein, 50cm, iron oxides | -6.739435 | 33.205022 | 1 | 2 | |
| ZX 257 | micro-vein, 5cm, iron oxides | -6.740807 | 33.205702 | 20 | 25 | |
| ZX 258 | micro-vein, 7cm, iron oxides | -6.743751 | 33.205864 | 29 | 12 | |
| ZX 259 | micro-vein, 6cm, iron oxides | -6.742865 | 33.203909 | 14 | 11 | |
| ZX 260 | major vein, quartz Iron oxides | -6.741219 | 33.202049 | 88 | 127 | |
| ZX 261 | major vein, 30cm, iron oxides | -6.740765 | 33.201968 | 36 | 14 | |
| ZX 262 | micro-vein, 8cm, iron oxides | -6.743916 | 33.202034 | 35 | 9 | |
| ZX 263 | micro-vein network, tension gash, iron oxides, 60cm | -6.753387 | 33.187545 | 15 | 6 | |
| ZX 264 | quartz vein, iron oxides, w, 40cm | -6.752773 | 33.187670 | 98 | 1570 | |
| ZX 265 | micro-vein array, iron oxides, 20cm | -6.751675 | 33.187140 | 161 | 189 | |
| ZX 266 | major vein, forming a 3m wide coridor with micro-veins | -6.751465 | 33.186288 | 27 | 491 | |
| ZX 267 | micro-vein, 20cm | -6.752114 | 33.186712 | 8 | 406 | |
| ZX 268 | granite,coarse, pink | -6.752111 | 33.186756 | 18 | 12 | |
| ZX 269 | granite,coarse, pink | -6.751999 | 33.186918 | 15 | 5 | |
| ZX 270 | micro-veins in a fault coridor, 0,5m | -6.742004 | 33.174568 | 6 | 3 | |
| ZX 271 | major vein, high content of iron oxides, 0,8m | -6.742474 | 33.172772 | 4 | 11 | |
| ZX 272 | major vein, high content of Iron oxides, 0,7m | -6.742111 | 33.171149 | 19 | 1205 | |
| ZX 273 | quartz vein, iron oxidation, 2,5cm | -6.750350 | 33.201670 | 21 | 6 | |
| ZX 274 | major vein, 3-10cm | -6.749790 | 33.200250 | 60 | 257 | |
| ZX 275 | 4 quartz veins @ 2cm | -6.749570 | 33.200250 | 83 | 26 | |
| ZX 276 | major vein, 8cm | -6.748580 | 33.200160 | 92 | 32 | |
| ZX 277 | major vein, w, 38cm | -6.749280 | 33.200050 | 117 | 1815 | |
| ZX 278 | quartz vein, iron oxides, granite | -6.748480 | 33.200060 | 753 | 1655 | |
| ZX 279 | micro-vein, in pink granite | -6.749910 | 33.202300 | 17 | 19 |
evresources.com.au
311-313 Hay St Subiaco, Western Australia 6008 +61 (0) 8 6489 0600 [email protected]
| Sample No. |
Description | Easting | Northing | Sn | W | |
| w= wolframite; sch= scheelite; fsp= feldspar | X | Y | ppm | ppm | ||
| ZX 280 | major quartz vein, 300cm, no visible mineralisation | -6.736111 | 33.172500 | 1 | 1 | |
| ZX 281 | major vein, 50cm | -6.736389 | 33.117222 | 1 | 6 | |
| ZX 282 | major vein, 80cm | -6.737500 | 33.173056 | 3 | 73 | |
| ZX 283 | major vein, 50cm, rare w | -6.737778 | 33.174167 | 1 | 912 | |
| ZX 284 | micro-vein, 4cm, rare w | -6.740000 | 33.175000 | 125 | 715 | |
| ZX 285 | micro-vein, 3cm, in pink granite with high K feldspar content | -6.739444 | 33.175833 | 34 | 6 | |
| ZX 286 | major vein, 80cm | -6.740833 | 33.176111 | 23 | 19 | |
| ZX 287 | major vein, 20cm | -6.741111 | 33.175278 | 21 | 9 | |
| ZX 288 | quartz vein, 12cm, iron oxides | -6.741667 | 33.175000 | 25 | 7 | |
| ZX 289 | micro-vein, 4cm, rare w, iron oxides | -6.738056 | 33.174444 | 1155 | 433 | |
| ZX 290 | quartz vein, 40cm, iron oxides | -6.736912 | 33.203347 | 12 | 6 | |
| ZX 291 | quartz vein, 40cm, iron oxides | -6.738216 | 33.205273 | 11 | 26 | |
| ZX 292 | quartz vein, 30cm, iron oxides | -6.739999 | 33.205743 | 1 | 4 | |
| ZX 293 | micro-veins of 2-10cm, iron oxides | -6.740706 | 33.206817 | 4 | 11 | |
| ZX 294 | quartz vein, 12cm, iron oxides | -6.742082 | 33.207037 | 1 | 2 | |
| ZX 295 | micro-vein, 5cm, w, iron oxides | -6.744477 | 33.204394 | 650 | 14950 | |
| ZX 296 | quartz vein, 8cm, iron oxides | -6.744319 | 33.203309 | 15 | 18 | |
| ZX 297 | quartz vein, 8cm, w, sulphides and iron oxides | -6.742508 | 33.200762 | 4310 | 8000 | |
| ZX 298 | quartz vein, 15cm, w, iron oxides | -6.740838 | 33.199831 | 8 | 5810 | |
| ZX 299 | major vein, 100cm | -6.738256 | 33.200107 | 72 | 260 | |
| ZX 300 | micro-veins of 2cm, iron oxides | -6.749131 | 33.185375 | 15 | 4 | |
| ZX 301 | micro-veins of 2cm, iron oxides | -6.748813 | 33.184858 | 134 | 12 | |
| ZX 302 | micro-veins of 2-3cm, iron oxides | -6.747790 | 33.183889 | 175 | 59 | |
| ZX 303 | quartz vein, 30cm, w, iron oxides | -6.746493 | 33.184126 | 189 | 1970 | |
| ZX 304 | micro-vein, 3-9cm, w, chalcopyrite, azurite and iron oxides | -6.747340 | 33.183053 | 264 | 4000 | |
| ZX 305 | major vein, 180cm, massive w, iron oxides | -6.748271 | 33.179430 | 2630 | 15900 0 |
|
| ZX 306 | quartz vein, 25cm, pyrite, chalcopyrite and iron oxides | -6.744883 | 33.177249 | 663 | 94 | |
| ZX 307 | major vein, 80cm, iron oxides | -6.744042 | 33.177989 | 30 | 119 | |
| ZX 308 | micro-vein, 2cm, iron oxides | -6.747292 | 33.181480 | 690 | 92 | |
| ZX 309 | micro-vein, 2cm, iron oxides | -6.746516 | 33.181688 | 98 | 23 | |
| ZX 310 | micro-vein, 5cm, K feldspar and iron oxides | -6.744159 | 33.178783 | 10 | 6 | |
| ZX 311 | micro-veins of 3-4cm, pyrite, chalcopyrite, azurite and iron oxides | -6.745295 | 33.177388 | 32 | 54 | |
| ZX 312 | quartz vein, 25cm, iron oxides | -6.746670 | 33.175879 | 27 | 11 | |
| ZX 313 | micro-veins, total of 45cm, iron oxides, cross-cutting each other, sinistral |
-6.748222 | 33.174172 | 22 | 14 | |
| ZX 314 | major vein, 180cm, iron oxides | -6.747977 | 33.172855 | 8 | 121 | |
| ZX 315 | quartz vein, w, 25cm, iron oxides | -6.750173 | 33.173065 | 465 | 3590 | |
| ZX 316 | granite between 2 quartz veins | -6.741982 | 33.171043 | 14 | 7 | |
| ZX 317 | major vein, high content of iron oxides, 0,6m | -6.741949 | 33.170333 | 574 | 75 | |
| ZX 318 | major vein of quartz with high content of Iron oxides, 0,7m | -6.745314 | 33.169805 | 1715 | 77 | |
| ZX 319 | massive quartz next to contact with granite, less iron oxides | -6.748245 | 33.169708 | 2 | 2 | |
| ZX 320 | system of quartz veins, on average of 4cm, iron oxides | -6.765477 | 33.201709 | 1 | 4 | |
| ZX 321 | major vein, iron oxides, Intense hydrothermal alteration, 40cm | -6.766519 | 33.201956 | 6 | 4 | |
| ZX 322 | tension gash filled with grey quartz and iron oxides, 5cm, length of gash 30cm |
-6.767579 | 33.201594 | 4 | 8 | |
| ZX 323 | major vein, iron oxides, Intense hydrothermal alteration, 100cm | -6.768272 | 33.201685 | 6 | 3 | |
| ZX 324 | major vein, malachite, iron oxides, intense hydrothermal alteration, 80cm |
-6.769017 | 33.202193 | 343 | 26 | |
| ZX 325 | tension gash filled with grey quartz and iron oxides, 15cm, length of 30cm |
-6.769398 | 33.201269 | 15 | 3 | |
| ZX 326 | granite host rock | -6.764556 | 33.201630 | 16 | 4 | |
| ZX 327 | granite host rock | -6.763329 | 33.201487 | 22 | 9 |
evresources.com.au
311-313 Hay St Subiaco, Western Australia 6008 +61 (0) 8 6489 0600 [email protected]
| Sample No. |
Description | Easting | Northing | Sn | W | |
| w= wolframite; sch= scheelite; fsp= feldspar | X | Y | ppm | ppm | ||
| ZX 328 | quartz vein, w, iron oxides, 10cm | -6.765805 | 33.203000 | 45 | 8390 | |
| ZX 329 | large gash filled with grey quartz, w, hydrothermal alteration, 30cm, length of 2,5 m |
-6.766820 | 33.203101 | 27 | 8530 | |
| ZX 330 | quartz vein, iron oxides, traces of dark mineral, 6cm | -6.766567 | 33.203624 | 5 | 57 | |
| ZX 331 | 2 parallel quartz veins 15cm from each other, iron oxides, 10cm each vein |
-6.767169 | 33.203277 | 3 | 6 | |
| ZX 332 | major vein, brecciated, iron oxides, 80cm | -6.768180 | 33.203598 | 9 | 3 | |
| ZX 333 | major vein, brecciated, iron oxides, 95cm | -6.768718 | 33.203570 | 10 | 4 | |
| ZX 334 | major vein, iron oxides, 100cm | -6.769525 | 33.204331 | 30 | 5 | |
| ZX 335 | major vein, fractured grey quartz, and brecciated iron oxides, 80cm | -6.768163 | 33.204735 | 127 | 6 | |
| ZX 336 | major vein, fractured grey quartz, and brecciated iron oxides, 80cm | -6.767652 | 33.204690 | 124 | 27 | |
| ZX 337 | major vein, hydrothermal alteration, 100cm | -6.767482 | 33.203916 | 20 | 27 | |
| ZX 338 | major vein, high content of iron oxides | -6.750721 | 33.170039 | 6 | 10 | |
| ZX 339 | sand with black mineral grains | -6.748840 | 33.199053 | 17 | 11 | |
| ZX 340 | major vein, iron oxides and some w, 30cm, | -6.762154 | 33.200506 | 898 | 3730 | |
| ZX 341 | major vein, iron oxides and rare w, 10cm, | -6.762075 | 33.199421 | 10 | 214 | |
| ZX 342 | quartz vein, w, 4cm | -6.761687 | 33.198188 | 1455 | 1615 | |
| ZX 343 | major vein, iron oxides, some w, 15-20cm | -6.761269 | 33.197635 | 670 | 2830 | |
| ZX 344 | major vein, white quartz, 4-6m | -6.762444 | 33.196604 | 5 | 11 | |
| ZX 345 | major vein, 2m | -6.763623 | 33.196410 | 117 | 9 | |
| ZX 346 | major vein, malachite, w, 15cm | -6.762600 | 33.199005 | 3420 | 31700 | |
| ZX 347 | major vein, 20cm | -6.762912 | 33.199650 | 74 | 444 | |
| ZX 348 | granite host rock | -6.762829 | 33.200419 | 20 | 15 | |
| ZX 349 | quartz vein, 8cm | -6.761961 | 33.201268 | 19 | 1365 | |
| ZX 350 | major vein, 50cm | -6.762813 | 33.203177 | 3 | 9 | |
| ZX 351 | quartz vein 3cm | -6.763347 | 33.203886 | 14 | 12 | |
| ZX 352 | quartz vein network of 2-3cm in microgranular granite | -6.763559 | 33.204728 | 14 | 4 | |
| ZX 353 | quartz vein, 4cm | -6.764421 | 33.205649 | 9 | 6 | |
| ZX 354 | quartz vein, black unidentified mineral, 8cm | -6.764510 | 33.207438 | 12 | 6 | |
| ZX 355 | major vein, oxides, malachite, 80cm | -6.772020 | 33.210091 | 22 | 6 | |
| ZX 356 | major vein with dark quartz, 50cm | -6.773462 | 33.211216 | 6 | 3 | |
| ZX 357 | 3 veins of 10-15cm each | -6.772508 | 33.211784 | 1 | 5 | |
| ZX 358 | major vein, tectonised, oxides in pink granite | -6.773095 | 33.214593 | 22 | 5 | |
| ZX 359 | major vein with dark quartz, 1m | -6.774627 | 33.211903 | 5 | 4 | |
| ZX 360 | major vein, iron oxides, 400m length | -6.740120 | 33.176240 | 28 | 12 | |
| ZX 361 | major vein, 30cm | -6.741220 | 33.176820 | 15 | 82 | |
| ZX 362 | major vein, 2m, in pink granite | -6.742450 | 33.177360 | 21 | 25 | |
| ZX 363 | micro-vein,3-4cm, 2m in length | -6.746640 | 33.176610 | 16 | 7 | |
| ZX 364 | quartz vein, 3-4cm, 2m in length | -6.747400 | 33.175420 | 16 | 4 | |
| ZX 365 | quartz vein, 3-4cm, 2m in length | -6.746550 | 33.175630 | 29 | 15 | |
| ZX 366 | quartz vein, 2-4cm, 40m in length | -6.745890 | 33.175520 | 27 | 7 | |
| ZX 367 | quartz vein, 1-2cm, 10m in length | -6.748420 | 33.203110 | 31 | 17 | |
| ZX 368 | quartz vein, 2-20cm, 20m in length | -6.747810 | 33.202790 | 714 | 814 | |
| ZX 369 | 4 quartz veins, 5cm each, iron oxides | -6.743710 | 33.174650 | 86 | 13 | |
| ZX 370 | quartz vein, iron oxides, w, 1-2cm, 10m in length | -6.746580 | 33.202330 | 431 | 1525 | |
| ZX 371 | quartz veins, iron oxides, w, 2-20cm, 5m in length | -6.747390 | 33.202310 | 325 | 322 | |
| ZX 372 | quartz veins, iron oxides, 2-4cm, 5m in length | -6.748740 | 33.202210 | 19 | 18 | |
| ZX 373 | quartz veins, iron oxides, <2cm, 10m in length | -6.746530 | 33.201370 | 27 | 4 | |
| ZX 374 | pink granite | -6.755797 | 33.188530 | 22 | 11 | |
| ZX 375 | two-mica granite | -6.748855 | 33.172907 | 13 | 4 |
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311-313 Hay St Subiaco, Western Australia 6008 +61 (0) 8 6489 0600 [email protected]
| Sample No. |
Description | Easting | Northing | Sn | W | |
| w= wolframite; sch= scheelite; fsp= feldspar | X | Y | ppm | ppm | ||
| ZX 376 | major vein, iron oxides | -6.748855 | 33.172907 | 54 | 439 | |
| ZX 410 | quartz vein, 5cm, w traces | -6,775634 | 33,224697 | 10 | 530 | |
| ZX 411 | major vein, 15cm, iron oxides | -6,774133 | 33,223148 | 2 | 4 | |
| ZX 412 | major vein, 10cm, w traces | -6,776979 | 33,223003 | 4 | 103 | |
| ZX 413 | major vein, 10cm, rich in iron oxides | -6.772690 | 33.221672 | 23 | 5 | |
| ZX 414 | major vein, 20cm, rich in iron oxides | -6.768264 | 33.222941 | 13 | 9 | |
| ZX 415 | micro-vein, 6cm, black mineral grains and oxides | -6.766240 | 33.215235 | 2 | 2 | |
| ZX 416 | major vein, 40cm, ion oxides | -6.773613 | 33.217851 | 7 | 6 | |
| ZX 417 | intersection of N90E major vein (10cm) and minor vein (8cm) oriented N50E |
-6.779446 | 33.217680 | 12 | 26 | |
| ZX 418 | quartz vein, 8cm | -6.770537 | 33.212522 | 2 | 2 | |
| ZX 419 | major vein, brecciated, 3m, black mineral grains and iron oxides | -6.775798 | 33.213780 | 1 | 3 | |
| ZX 420 | major vein, 12cm, black mineral grains, brecciated | -6.771011 | 33.209723 | 3 | 12 | |
| ZX 421 | major vein, 150cm, black mineral grains and iron oxides | -6.765299 | 33.201699 | 1 | 2 | |
| ZX 422 | major vein, 3m, black mineral grains, iron oxides, malachite traces | -6.757143 | 33.206650 | 351 | 73 | |
| ZX 423 | major vein, 12cm, w | -6.755457 | 33.203717 | 1740 | 1205 | |
| ZX 424 | major vein, 1m, abundant w, iron oxides, malachite traces | -6.758466 | 33.201869 | 5480 | 34900 | |
| ZX 425 | major vein, 1m, massive w | -6.759260 | 33.198460 | 7210 | 15900 0 |
|
| ZX 426 | major vein, 80cm, w, iron oxides | -6.758270 | 33.200124 | 410 | 36500 | |
| ZX 427 | major vein, 60cm | -6.757128 | 33.201187 | 42 | 22 | |
| ZX 428 | major vein, 50cm, w, iron oxides | -6.740836 | 33.199873 | 50 | 14700 0 |
|
| ZX 429 | major vein, 60cm, iron oxides | -6.738289 | 33,199567 | 5 | 30 | |
| ZX 430 | major vein, 12cm, oxides, minor scheelite | -6.747485 | 33.182598 | 1 | 57 | |
| ZX 431 | major vein, 1m, w, iron oxides | -6.754869 | 33.180223 | 1240 | 8970 | |
| ZX 432 | minor vein, 5cm | -6.754869 | 33.180223 | 359 | 48 | |
| ZX 433 | minor vein, 5cm, brecciated | -6.765633 | 33.190761 | 6 | 12 | |
| ZX 434 | major vein, 5cm, brecciated | -6.762340 | 33.191810 | 659 | 63 | |
| ZX 435 | minor vein, 5cm, brecciated | -6.763670 | 33.192355 | 45 | 11 | |
| ZX 436 | major vein, 5cm, brecciated | -6.764369 | 33.192088 | 70 | 37 | |
| ZX 437 | major vein, 12cm | -6.792124 | 33.212602 | 6 | 10 | |
| ZX 438 | quartz vein, 8cm | -6.791157 | 33.211362 | 3 | 8 | |
| ZX 439 | major vein, 12cm | -6.792222 | 33.209935 | 443 | 15 | |
| ZX 440 | quartz vein, 5cm | -6.789157 | 33.212477 | 4 | 10 | |
| ZX 441 | quartz vein, 4cm | -6.787395 | 33.212489 | 5 | 5 | |
| ZX 442 | major vein, 10cm | -6.781785 | 33.215945 | 3 | 4 | |
| ZX 443 | major vein, 50cm | -6.782194 | 33.217869 | 3 | 6 | |
| ZX 444 | major vein, 10cm | -6.783863 | 33.218696 | 4 | 7 | |
| ZX/G01 | quartz vein | -6.752336 | 33.199047 | 126 | 67 | |
| ZX/G02 | quartz vein | -6.752336 | 33.199047 | 31 | 8 | |
| ZX/G03 | quartz vein | -6.752336 | 33.199047 | 29 | 18 | |
| ZX/G04 | quartz vein | -6.752336 | 33.199047 | 76 | 52 | |
| ZX/G05 | quartz vein | -6.752336 | 33.199047 | 16 | 7 | |
| ZX/G06 | quartz vein | -6.752336 | 33.199047 | 32 | 5 | |
| ZX/G07 | quartz vein | -6.752336 | 33.199047 | 82 | 63 | |
| ZX/G08 | quartz vein | -6.752336 | 33.199047 | 35 | 390 | |
| ZX/G09 | quartz vein | -6.752336 | 33.199047 | 50 | 15 | |
| ZX/G10 | quartz vein | -6.752336 | 33.199047 | 24 | 14 | |
| ZX/G11 | quartz vein | -6.752336 | 33.199047 | 48 | 873 | |
| ZX/G12 | quartz vein | -6.752336 | 33.199047 | 17 | 14 |
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311-313 Hay St Subiaco, Western Australia 6008 +61 (0) 8 6489 0600 [email protected]
| Sample No. |
Description | Easting | Northing | Sn | W | |
| w= wolframite; sch= scheelite; fsp= feldspar | X | Y | ppm | ppm | ||
| ZX/G13 | quartz vein | -6.752336 | 33.199047 | 680 | 45900 | |
| ZX/G14 | quartz vein | -6.752336 | 33.199047 | 343 | 2120 | |
| ZX/G15 | quartz vein | -6.752336 | 33.199047 | 325 | 6370 | |
| ZX/G16 | quartz vein | -6.752336 | 33.199047 | 890 | 42800 | |
| ZX/G17 | quartz vein | -6.752336 | 33.199047 | 41 | 362 | |
| ZX/G18 | quartz vein | -6.752336 | 33.199047 | 90 | 20000 | |
| ZX/G19 | quartz vein | -6.752336 | 33.199047 | 282 | 5290 | |
| ZX/G20 | quartz vein | -6.752336 | 33.199047 | 310 | 13250 | |
| ZX/G21 | quartz vein | -6.752336 | 33.199047 | 160 | 17050 | |
| ZX/G22 | quartz vein | -6.752336 | 33.199047 | 626 | 4260 | |
| ZX/G23 | quartz vein | -6.752336 | 33.199047 | 2740 | 2610 | |
| ZX/G24 | quartz vein | -6.752336 | 33.199047 | 117 | 123 | |
| ZX/G25 | quartz vein | -6.752336 | 33.199047 | 18 | 10 | |
| ZX/G26 | quartz vein | -6.752336 | 33.199047 | 16 | 7 | |
| ZX/G27 | quartz vein | -6.752336 | 33.199047 | 29 | 25 | |
| ZX/G28 | quartz vein | -6.752336 | 33.199047 | 51 | 58 | |
| ZX/G29 | quartz vein | -6.752336 | 33.199047 | 184 | 220 | |
| ZX/G30 | quartz vein | -6.752336 | 33.199047 | 37 | 36 |
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311-313 Hay St Subiaco, Western Australia 6008 +61 (0) 8 6489 0600 [email protected]
JORC Code, 2012 Edition – Table 1 report template
Section 1 Sampling Techniques and Data
(Criteria in this section apply to all succeeding sections.)
| Criteria | JORC Code explanation | Commentary |
|---|---|---|
| Sampling techniques |
• Nature and quality of sampling (e.g., cut channels, random chips, or specific specialised industry standard measurement tools appropriate to the minerals under investigation, such as down hole gamma sondes, or handheld XRF instruments, etc.). These examples should not be taken as limiting the broad meaning of sampling. • Include reference to measures taken to ensure sample representivity and the appropriate calibration of any measurement tools or systems used. • Aspects of the determination of mineralisation that are Material to the Public Report. • In cases where ‘industry standard’ work has been done this would be relatively simple (e.g., ‘reverse circulation drilling was used to obtain 1 m samples from which 3 kg was pulverised to produce a 30 g charge for fire assay’). In other cases, more explanation may be required, such as where there is coarse gold that has inherent sampling problems. Unusual commodities or mineralisation types (e.g., submarine nodules) may warrant disclosure of detailed information. |
• A raw target mass of averaged 1.5 kg (1 – 2 kg) was taken from the surface (fresh granite, quartz vein and veinlets), and from an underground gallery (fresh granite, quartz vein) • Quartz vein material frequently with visible mineralization (wolframite), granite and micro quartz veins from surface and underground frequently without visible mineralisation |
| Drilling techniques |
• Drill type (e.g., core, reverse circulation, open-hole hammer, rotary air blast, auger, Bangka, sonic, etc.) and details (e.g., core diameter, triple or standard tube, depth of diamond tails, face-sampling bit or other type, whether core is _oriented and if so, by what method, etc.). _ |
• No drilling was performed |
| Drill sample recovery |
• Method of recording and assessing core and chip sample recoveries and results assessed. • Measures taken to maximise sample recovery and ensure representative nature of the samples. • Whether a relationship exists between sample recovery and grade and whether sample bias may have occurred due to preferential loss/gain of fine/coarse material. |
• No drilling was performed |
| Logging | • Whether core and chip samples have been geologically and geotechnically logged to a level of detail to support appropriate Mineral Resource estimation, mining studies and metallurgical studies. • Whether logging is qualitative or quantitative in nature. Core (or costean, _channel, etc.) photography. _ |
• No drilling was performed |
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311-313 Hay St Subiaco, Western Australia 6008 +61 (0) 8 6489 0600 [email protected]
| Criteria | JORC Code explanation | Commentary | |
| • The total length andpercentage of the relevant intersections logged. |
|||
| Sub-sampling techniques and sample preparation |
• If core, whether cut or sawn and whether quarter, half or all core taken. • If non-core, whether riffled, tube sampled, rotary split, etc. and whether sampled wet or dry. • For all sample types, the nature, quality and appropriateness of the sample preparation technique. • Quality control procedures adopted for all sub-sampling stages to maximise representivity of samples. • Measures taken to ensure that the sampling is representative of the in-situ material collected, including for instance results for field duplicate/second-half sampling. • Whether sample sizes are appropriate to the grain size of the material being sampled. |
• Rock samples were dry • Comminution and preparation to sub-samples (pulps) was conducted at SGS facility at Mohammedia in Morocco, using SGS preparation method (PRP89) • Weight and dry sample • Crush entire sample to -2mm to 75% • Split around 220-250gr using riffle splitter • Pulverize the 220-250gr to 85% -75 microns • Ship of around 70-100gr to ALS Seville (Spain), where a new QAQC control of pulps was performed by PUL-31 to ascertain the minimum pulp size (pulverise total sample to 85% passing 75 micron) • Due to the early stage of exploration (sampling was done reconnaissance style), control samples (standards, blanks and both field and lab duplicates) were not inserted, However, both ALS and SGS are internationally accredited and well-regarded laboratories that apply internal QAQC procedures. ALS by default introduces blanks, duplicates and standards during the execution of the assaying programme • Sample size at Christina Project is believed to be broadly appropriate and consistent with industry best-practice. But given the high level of heterogeneity in tungsten mineralization in quartz veins, the sample sizes used for assessment of W grades in rock samples at Christina are too small and hence a reliable assessment of the W grade is not possible |
|
| Quality of assay data and laboratory tests |
• The nature, quality and appropriateness of the assaying and laboratory procedures used and whether the technique is considered partial or total. • For geophysical tools, spectrometers, handheld XRF instruments, etc., the parameters used in determining the analysis including instrument make and model, reading times, calibrations factors applied and their derivation, etc. • Nature of quality control procedures adopted (e.g., standards, blanks, duplicates, external laboratory checks) and whether acceptable levels of accuracy (i.e., lack of bias) and precision have been established. |
• Assaying conducted by ALS Ireland • All 339 samples analysed by Lithium Borate Fusion ICP-MS (ME- MS81) • Assay results in excess of 1% for W and Sn were re-assayed by ME-XRF1 5b • Sample preparation process and analytical methods are standard for W-Sn deposits worldwide • Standard quality procedures by ALS (standards, blanks, duplicates) |
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| Criteria | JORC Code explanation | Commentary | |
| Verification of sampling and assaying |
• The verification of significant intersections by either independent or alternative company personnel. • The use of twinned holes. • Documentation of primary data, data entry procedures, data verification, data storage (physical and electronic) protocols. • Discuss any adjustment to assay data. |
• No drilling was performed |
|
| Location of data points |
• Accuracy and quality of surveys used to locate drill holes (collar and down- hole surveys), trenches, mine workings and other locations used in Mineral Resource estimation. • Specification of the grid system used. • Quality and adequacy of topographic control. |
• Sample points recorded by GPS (NAVA F30) • Grid system: WGS-84 |
|
| Data spacing and distribution |
• Data spacing for reporting of Exploration Results. • Whether the data spacing and distribution is sufficient to establish the degree of geological and grade continuity appropriate for the Mineral Resource and Ore Reserve estimation procedure(s) and classifications applied. • Whether sample compositing has been applied. |
• The samples are reconnaissance in nature, and therefore sampling spacing is very variable. Sample spacing over areas with a high density of quartz veining is higher than over areas with little quartz veining • The data is not suitable for use in mineral resource estimate reporting and is not intended for such use |
|
| Orientation of data in relation to geological structure |
• Whether the orientation of sampling achieves unbiased sampling of possible structures and the extent to which this is known, considering the deposit type. • If the relationship between the drilling orientation and the orientation of key mineralised structures is considered to have introduced a sampling bias, this should be assessed and reported if material. |
• The samples are reconnaissance in nature and cover different locations, so any biasing effect caused by orientation is yet to be determined |
|
| Sample security |
• The measures taken to ensure sample security. |
• Between sampling and time of delivery at SGS Mohammedia samples were stored for two weeks at home of EV Resources consultant Rachid El Moukhayar |
|
| Audits or reviews |
• The results of any audits or reviews of sampling techniques and data. |
• No audits have been carried out at this point |
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Section 2 Reporting of Exploration Results
(Criteria listed in the preceding section also apply to this section.)
| Criteria | JORC Code explanation | Commentary |
|---|---|---|
| Mineral tenement and land tenure status |
• Type, reference name/number, location and ownership including agreements or material issues with third parties such as joint ventures, partnerships, overriding royalties, native title interests, historical sites, wilderness or national park and environmental settings. • The security of the tenure held at the time of reporting along with any known impediments to obtaining a licence to operate in the area. |
• Permit No. PR2137940, PR2137970 and PR1137830. The licences are exploration licences, with an application for the conversion of a portion to an exploitation licence • No material issues with third parties • The project area is located ca 120 km east of the coastal city of Casablanca |
| Exploration done by other parties |
• Acknowledgment and appraisal of exploration by other parties. |
• There has been no previous conventional exploration |
| Geology | • Deposit type, geological setting and style of mineralisation. |
• Hercynian vein-type mineralisation hosted in two-mica granite |
| Drill hole Information |
• A summary of all information material to the understanding of the exploration results including a tabulation of the following information for all Material drill holes: o easting and northing of the drill hole collaro elevation or RL (Reduced Level – elevation above sea level in meters) ofthe drill hole collar o dip and azimuth of the holeo down hole length and interception deptho hole length.• If the exclusion of this information is justified on the basis that the information is not Material and this exclusion does not detract from the understanding of the report, the Competent Person should clearly explain why this is the case. |
• No drilling was performed |
| Data aggregation methods |
• In reporting Exploration Results, weighting averaging techniques, maximum and/or minimum grade truncations (e.g., cutting of high grades) and cut-off grades are usually Material and should be stated. • Where aggregate intercepts incorporate short lengths of high-grade results and longer lengths of low-grade results, the procedure used for such aggregation should be stated and some typical examples of such aggregations should be shown in detail. |
• No data aggregation methods were used in this announcement |
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311-313 Hay St Subiaco, Western Australia 6008 +61 (0) 8 6489 0600 [email protected]
| Criteria | JORC Code explanation | Commentary | |
| • The assumptions used for any reporting of metal equivalent values should be _clearly stated. _ |
|||
| Relationship between mineralisation widths and intercept lengths |
• These relationships are particularly important in the reporting of Exploration Results. • If the geometry of the mineralisation with respect to the drill hole angle is known, its nature should be reported. • If it is not known and only the down hole lengths are reported, there should be a clear statement to this effect (e.g., ‘down hole length, true width not _known’). _ |
• No drilling was performed |
|
| Diagrams | • Appropriate maps and sections (with scales) and tabulations of intercepts should be included for any significant discovery being reported. These should include, but not be limited to a plan view of drill hole collar locations and _appropriate sectional views. _ |
• No drilling was performed |
|
| Balanced reporting |
• Where comprehensive reporting of all Exploration Results is not practicable, representative reporting of both low and high grades and/or widths should be _practiced to avoid misleading reporting of Exploration Results. _ |
• All assay results (and QA/QC) of this campaign are reported in ALS Report 13 February 2023 |
|
| Other substantive exploration data |
• Other exploration data, if meaningful and material, should be reported including (but not limited to): geological observations; geophysical survey results; geochemical survey results; bulk samples – size and method of treatment; metallurgical test results; bulk density, groundwater, geotechnical and rock characteristics; potential deleterious or contaminating substances. |
• No information available on metallurgy, ground water, bulk density, or rock stability |
|
| Further work | • The nature and scale of planned further work (e.g., tests for lateral extensions or depth extensions or large-scale step-out drilling). • Diagrams clearly highlighting the areas of possible extensions, including the main geological interpretations and future drilling areas, provided this information is not commercially sensitive. |
• An initial reconnaissance-style diamond drilling programme of 2,500m has been planned in areas with high assay values and with a high density of quartz veining, and is waiting for execution during Q2 2023 • Further synthesise results of geological and structural mapping campaign, e.g., wolframite mineralisation in quartz veins and micro veins away from well-known areas of historical mining |
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311-313 Hay St Subiaco, Western Australia 6008 +61 (0) 8 6489 0600 [email protected]